This likely influences geographic variation in surface nutrient availability, and therefore
stable isotope ratios in POM, primary producers [12] and consumers [14].
Early TRL projects focused on establishing long tree - ring records from temperature - sensitive boreal forest locations in North American for studies of global change, using dendrochronologically dated wood, to investigate the value of
stable isotope ratios in cellulose as paleo - thermometers and developing the necessary computer software for processing the data.
Stable isotope ratios in atmospheric methane and carbon dioxide provide a window on the sources as well.
The team found that the degree of nitrogen pollution, which is worsening in urban areas, can be evaluated by analyzing the nitrogen content and
the stable isotope ratio in bryophytes.
Not exact matches
Using spectroscopy,
stable isotope ratios (carbon, nitrogen and sulphur) were investigated
in the collagen of the bones, along with the
ratio of strontium to calcium
in the bone mineral.
Researchers linked dated graffiti about droughts
in a cave
in China to physical evidence
in the cave of the water shortages, such as changes
in ratios of
stable isotopes in specific layers of stalagmites
«Laser ablation
isotope ratio mass spectrometry for enhanced sensitivity and spatial resolution
in stable isotope analysis.»
Qualitatively, the slow ventilation is consistent with very saline and very cold deep waters reconstructed for the last glacial maximum (Adkins et al., 2002), as well as low glacial
stable carbon
isotope ratios (13C / 12C)
in the deep South Atlantic.
Comparison of
stable carbon
isotope ratios in the whole wood, cellulose and lignin of oak tree - rings Dr. Ron Towner from the Laboratory of Tree - Ring Research at the University of Arizona explains the principles behind dendrochronology and why this dating
It basically says that ringwidth is a function of: age trend + climate signal + endogenous (local) disturbances + exogenous (standwide) disturbances + unexplained variation Basically, this concept also underlies all other dendro proxies, be it maximum latewood density or
stable isotope ratios, even though there are variations, e. g. age trend
in density data is treated differently from ring width data).
This analytical document shows that
stable isotope ratios can be used to monitor changes
in the character of precipitation
in response to periodic variability or changes
in climate.
Stable carbon
isotope ratios from tree rings record changes
in the internal concentration of carbon dioxide and,
in the northern Boreal zone, are regarded as a proxy for photosynthetic rate, and therefore summer sunshine.
Stable oxygen
isotope ratios contained
in the shell can be used to infer past water temperatures.
This proxy, known as the δ18O
stable oxygen
isotope ratio, varies
in proportion to the ambient moisture.
The
ratio of
stable isotopes oxygen - 18 and oxygen - 16
in the foraminifera is an indicator of ocean temperature.
For example, extreme values of the
ratio of
stable isotopes in foraminifera from the eastern Pacific have previously been interpreted as ENSO activity, but modeling suggests that this interpretation may not always be suitable for past climates due to variability caused by other factors.
The size of the carbon injection is estimated from changes
in the
stable carbon
isotope ratio 13C / 12C
in sediments and from ocean acidification implied by changes
in the ocean depth below which carbonate dissolution occurred.